Impact of tourism on groundwater extraction on the island of
Transcription
Impact of tourism on groundwater extraction on the island of
Impact of tourism on groundwater extraction on the island of Langeoog, Germany Georg Houben Federal Institute for Geosciences and Natural Resources(BGR), Hannover, Germany [email protected] Water supply on the East Frisian Islands The East Frisian Islands are a chain of barrier islands in the Wadden Sea area of the North Sea. Extensive intertidal mudflats separate them from the coast. Baltic Sea North Sea N o r t h Hannover D s t a E CZ 0 200km Juist N s I s l a n d Wangerooge n s i a i r F Spiekeroog Langeoog Norderney CH S e a PL Niedersachsen NL F The island of Langeoog has three freshwater lenses. The separation was caused by storm flood inundations in historical times, especially during the 17th century. Baltrum Mellum n d d e a W S e a Ja Borkum SW de Rainwater infiltrating into the dunes forms freshwater lenses in dynamic equilibrium with surrounding saline water. Water supply on most islands depends on these lenses. Example Langeog Memmert Wittmund Leybucht elg Kaap dunes [Water work West] (m) 20 Jever ndz W E Wilhelmshaven Norden Ra NE W Melkhörn dunes Heerenhus dunes [Water work East] Kleine Große Schlopp Schlopp Eastern dunes (m) 20 Meierei sea level sea level at Aurich -30 -30 Jadebusen 0 water well fresh water 25 km 12.5 0 1 km saline water Groundwater extraction Borkum Juist Norderney Langeoog Spiekeroog Cross-section of the East Frisian coast (modified after Streif 1990) The economic base of the islands is tourism. The high seasonality of this business and the elevated water demand of tourists stress the limited water resources. Climate change might exacerbate this situation. [m³/a] Cross-section of the freshwater lenses of Langeoog (modified after Streif 1990). 800,000 300,000 940,000 334,000 140,000 Water supply solely depends on groundwater pumped from the western freshwater lens. To prevent upconing of underlying saline water, extraction is distributed over 20 shallow wells (10 to 18 m depth) which pump intermittently at low rates of around 10 m³/h. The islands Baltrum and Wangerooge are supplied from the mainland via pipeline Water demand Historical development Seasonal variations groundwater consumption groundwater extraction overnight stays 450 groundwater volume [m³/a x 1000] 3 400 3000 2800 2600 2400 2200 2000 1800 1600 1400 1200 1000 800 600 400 200 350 300 250 2 200 150 1 1 = post-war refugees 2 = water work East activated 3 = water work West shut down 100 50 0 1940 1950 1960 1970 1980 1990 2000 2010 The 2011 extraction of 334,000 m³/a is about a quarter less than the peak extraction of 452,000 m³/a recorded 1983, although the number of overnight stays has remained more or less stable at least since 1990! Water demand varies strongly according to seasons, vacation periods, public holidays and individual weekends. The lowest water demand on Langeoog during the off-season of 2011 was 238 m³/d while the maximum during the Easter holidays reached 1,894 m³/d, a factor of eight between maximum and minimum! 180 1500 160 140 1400 120 100 1300 15 14 13 12 11 10 9 8 7 1990 1995 2000 2005 2010 Guest numbers rise but the number of overnight stays remains constant = shorter vacations = more frequent cleaning of rooms and washing of towels and linen (5) (6) (1) 400 (?) (?) (7) (2) (1) 200 0 (3) 2000 1600 1200 Langeoog (4)(5) Qtot= 333,808 m³/a (6) (7) (1) (1) 800 0 Groundwater extraction on the islands of Spiekeroog and Langeoog in the year 2011 showing strong seasonal demand variation. Peaks 11 2011 2011 2011 2011 2011 2011 2011 2011 2011 2011 2011 2012 0 2 1. .02. .03. .04. .05. .06. .07. .08. .09. .10. .11. .12. .01. are even more pronounced on the smaller island of Spiekeroog. 0 . 01 01 01 01 01 01 01 01 01 01 01 01 01 After data by OOWV. Average monthly air temperature [°C] 1600 1,000 overnight stays per year 1,000 guests per year average overnight stays per guest guests overnight stays Qtot= 150,618 m³/a (3)(?) (4) = Ascencion (5) = Pentecost (6) = Unification Day (7) = Autumn break 400 Conclusions air temperature moving average (48 months) moving average (96 months) 25 1700 Spiekeroog 600 Climate change 220 200 800 At 125 liter per day and person, the 2,000 permanent residents consume about 92,000 m³/a. Subtracting this from 2011´s consumption, the remaining 242,000 m³/a, equivalent to about 72 % of all extraction, must be attributed to tourism. Tourism Langeoog 2011: (a) 2,000 permanent residents (b) 150 seasonal workers (c) 1,540,000 overnight stays (d) 124,000 day visitors (1) = X-mas/New Year (2) = Carnival (3) = Easter (4) 1000 Groundwater extraction [m³/d] 500 overnight stays per year [x 1000] Consumption steadily rose until the 1980s, parallel to increasing tourism. With the implementation of watersaving household appliances in the 1990s, consumption significantly decreased. 25 20 20 15 15 10 10 5 5 0 0 -5 -5 u u u u u -10 00 19 -10 10 19 20 19 30 19 40 19 50 19 60 19 70 19 80 19 90 19 00 20 10 20 Air temperature records from the island of Norderney indicate an increase of the average annual temperature of about 2.0° C over the last 115 years. Especially summers in the last 20 years have become warmer and cold winters have become less frequent. Will this cause an increase in water demand? u Water supply on East Frisian Islands mainly depends on freshwater lenses Tourisms accounts for more than 70% of all water consumption Strong demand variations over the course of the year due to tourist seasons Water consumption has decreased due to implementation of water saving installations although number of overnight stays has become constant Tendency towards more frequent but shorter vacations might increase demand again (more frequent washing and cleaning) Future effects of climate change (rising temperatures in summer) might be a game-changer. The results presented on this poster were elaborated in the framework of the BGR project FLIN (Freshwater Lens Investigations) References: Streif, H. 1990. Das ostfriesische Küstengebiet: Nordsee, Inseln, Watten und Marschen. Sammlung geologischer Führer 57, 376 p., Berlin. Acknowledgement: We thank the Oldenburgisch-Ostfriesischer Wasservernband (OOWV) for data on water consumption